{"title":"Hydrogeochemical response of aquifers to intensive groundwater pumping for rice-rice rotation","authors":"M.G. Mostofa Amin, Atiqur Rahman, Most. Sumiya Akter, Md. Mamun Rana, Md Shariot-Ullah","doi":"10.1016/j.gsd.2025.101485","DOIUrl":null,"url":null,"abstract":"<div><div>Extensive irrigated rice cultivation is often blamed for endangering groundwater resources. Therefore, the study aims to assess the hydro-geochemical properties of the geologic formation, investigate the hydro-geophysical impacts, and quantify the groundwater recharge and nutrient leaching potential, nutrient accumulation in geologic formation, and nutrient dynamics in the aquifers. Soil samples from the geologic formation were collected at 3-m intervals. Two observation wells were used to measure water level and nutrient dynamics. Field lysimeters assessed groundwater recharge potential and nutrient leaching. A test drilling and three pumping tests revealed that a 38-m clay layer separates an upper shallow aquifer from a deep confined aquifer (storage coefficient of 0.00051 and transmissibility of 2151 m<sup>2</sup>/day). Pumping tests resulted in a 0.8–1.1 m drawdown in the deep (pumping) aquifer, but an elastic subsidence of 5.7–9.1 mm caused a decrease in the water table depth of the shallow aquifer. Groundwater level peaked in October and followed a sharp decline during the Boro rice season (January–April) because of extraction for irrigation. The nutrient concentrations in the geologic layers (0.43–1.41 g N/kg and 4.02–32.16 mg P/kg) were relatively higher with higher clay content. Nitrogen levels in groundwater increased in the wet rice season and decreased in the dry season, whereas P was higher in the dry season due to varying transport and degradation rates. The rice fields had a huge groundwater recharge potential (38–74 % of water input) and moderate nutrient leaching (1–6.7 mg N/L and 0.05–0.63 mg P/L). However, nutrient concentrations in groundwater were sometimes even higher than the leaching concentrations. These results will help create an irrigation and nutrient management plan for rice cultivation. Increasing rainfed rice production would reduce the demand for irrigated Boro rice production and can have multifaceted positive effects on agricultural water security.</div></div>","PeriodicalId":37879,"journal":{"name":"Groundwater for Sustainable Development","volume":"30 ","pages":"Article 101485"},"PeriodicalIF":4.9000,"publicationDate":"2025-06-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Groundwater for Sustainable Development","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2352801X25000827","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENGINEERING, ENVIRONMENTAL","Score":null,"Total":0}
引用次数: 0
Abstract
Extensive irrigated rice cultivation is often blamed for endangering groundwater resources. Therefore, the study aims to assess the hydro-geochemical properties of the geologic formation, investigate the hydro-geophysical impacts, and quantify the groundwater recharge and nutrient leaching potential, nutrient accumulation in geologic formation, and nutrient dynamics in the aquifers. Soil samples from the geologic formation were collected at 3-m intervals. Two observation wells were used to measure water level and nutrient dynamics. Field lysimeters assessed groundwater recharge potential and nutrient leaching. A test drilling and three pumping tests revealed that a 38-m clay layer separates an upper shallow aquifer from a deep confined aquifer (storage coefficient of 0.00051 and transmissibility of 2151 m2/day). Pumping tests resulted in a 0.8–1.1 m drawdown in the deep (pumping) aquifer, but an elastic subsidence of 5.7–9.1 mm caused a decrease in the water table depth of the shallow aquifer. Groundwater level peaked in October and followed a sharp decline during the Boro rice season (January–April) because of extraction for irrigation. The nutrient concentrations in the geologic layers (0.43–1.41 g N/kg and 4.02–32.16 mg P/kg) were relatively higher with higher clay content. Nitrogen levels in groundwater increased in the wet rice season and decreased in the dry season, whereas P was higher in the dry season due to varying transport and degradation rates. The rice fields had a huge groundwater recharge potential (38–74 % of water input) and moderate nutrient leaching (1–6.7 mg N/L and 0.05–0.63 mg P/L). However, nutrient concentrations in groundwater were sometimes even higher than the leaching concentrations. These results will help create an irrigation and nutrient management plan for rice cultivation. Increasing rainfed rice production would reduce the demand for irrigated Boro rice production and can have multifaceted positive effects on agricultural water security.
期刊介绍:
Groundwater for Sustainable Development is directed to different stakeholders and professionals, including government and non-governmental organizations, international funding agencies, universities, public water institutions, public health and other public/private sector professionals, and other relevant institutions. It is aimed at professionals, academics and students in the fields of disciplines such as: groundwater and its connection to surface hydrology and environment, soil sciences, engineering, ecology, microbiology, atmospheric sciences, analytical chemistry, hydro-engineering, water technology, environmental ethics, economics, public health, policy, as well as social sciences, legal disciplines, or any other area connected with water issues. The objectives of this journal are to facilitate: • The improvement of effective and sustainable management of water resources across the globe. • The improvement of human access to groundwater resources in adequate quantity and good quality. • The meeting of the increasing demand for drinking and irrigation water needed for food security to contribute to a social and economically sound human development. • The creation of a global inter- and multidisciplinary platform and forum to improve our understanding of groundwater resources and to advocate their effective and sustainable management and protection against contamination. • Interdisciplinary information exchange and to stimulate scientific research in the fields of groundwater related sciences and social and health sciences required to achieve the United Nations Millennium Development Goals for sustainable development.